Chemical reactions at the mineral–solution interface control important interfacial processes, such as geochemical element cycling, nutrient recovery from eutrophicated waters, sequestration of toxic contaminants, and geological carbon storage by mineral carbonation. By time-resolved in situ imaging of nanoscale mineral interfacial reactions, it is possible to clarify the mechanisms governing mineral–fluid reactions.

中文翻译：

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通过原位原子力显微镜成像的环境矿物界面处的溶解和沉淀动力学。

矿物-溶液界面的化学反应控制着重要的界面过程，例如地球化学元素循环，富营养化水中的养分回收，有毒污染物的隔离以及矿物碳酸化作用的地​​质碳储量。通过时间分辨的纳米级矿物界面反应的原位成像，可以阐明控制矿物-流体反应的机理。